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contributor authorPolzin, Kurt L.
date accessioned2017-06-09T16:30:28Z
date available2017-06-09T16:30:28Z
date copyright2010/04/01
date issued2009
identifier issn0022-3670
identifier otherams-69115.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210749
description abstractThe issue of internal wave?mesoscale eddy interactions is revisited. Previous observational work identified the mesoscale eddy field as a possible source of internal wave energy. Characterization of the coupling as a viscous process provides a smaller horizontal transfer coefficient than previously obtained, with vh ? 50 m2 s?1 in contrast to ?h ? 200?400 m2 s?1, and a vertical transfer coefficient bounded away from zero, with ?? + (?f?2/N?2)Kh ? 2.5 ± 0.3 ? 10?3 m2 s?1 in contrast to ?? + (?f?2/N?2)Kh = 0 ± 2 ? 10?2 m2 s?1. Current meter data from the Local Dynamics Experiment of the PolyMode field program indicate mesoscale eddy?internal wave coupling through horizontal interactions (i) is a significant sink of eddy energy and (ii) plays an O(1) role in the energy budget of the internal wave field.
publisherAmerican Meteorological Society
titleMesoscale Eddy–Internal Wave Coupling. Part II: Energetics and Results from PolyMode
typeJournal Paper
journal volume40
journal issue4
journal titleJournal of Physical Oceanography
identifier doi10.1175/2009JPO4039.1
journal fristpage789
journal lastpage801
treeJournal of Physical Oceanography:;2009:;Volume( 040 ):;issue: 004
contenttypeFulltext


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